Deterioration-buckling failure mechanism of consequent bedding limestone bank slope in Three Gorges Reservoir area

In the Wuxia section of the Three Gorges Reservoir area, it is found that there are many deformation signs of sliding-bending along the bedding bank slope, and the cyclic fluctuation of reservoir water worsens the deterioration and instability of the bank leading edge. Taking Qingshi #6 slope in th...

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Main Authors: YAN Guo-qiang, YIN Yue-ping, HUANG Bo-lin, HU Lei
Format: Article
Language:English
Published: SCIENCE PRESS , 16 DONGHUANGCHENGGEN NORTH ST, BEIJING, PEOPLES R CHINA, 100717 2022-09-01
Series:Rock and Soil Mechanics
Subjects:
Online Access:http://rocksoilmech.whrsm.ac.cn/EN/10.16285/j.rsm.2021.7009
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author YAN Guo-qiang
YIN Yue-ping
HUANG Bo-lin
HU Lei
author_facet YAN Guo-qiang
YIN Yue-ping
HUANG Bo-lin
HU Lei
author_sort YAN Guo-qiang
collection DOAJ
description In the Wuxia section of the Three Gorges Reservoir area, it is found that there are many deformation signs of sliding-bending along the bedding bank slope, and the cyclic fluctuation of reservoir water worsens the deterioration and instability of the bank leading edge. Taking Qingshi #6 slope in the Wuxia section as an example, an laboratory generalized model is constructed to study the catastrophe mechanism of bedding limestone bank slope under the deterioration of rock mass in hydro-fluctuation belt. The research shows that: the bank slope is in a stable state as a whole for a long time before impoundment. After impoundment, with the deterioration aggravation of rock mass, the bank slope deformation intensifies until buckling failure. The deterioration of rock mass shortens the instability process of ‘deterioration-buckling’. Kinematic analysis shows that the peak velocity of the same rock stratum is similar during buckling failure. The movement characteristics of the rear part of the ‘buckling point’ of rock mass are relatively consistent, but the front part is relatively discrete. The buckling failure is the turning point and apex of bank slope energy release. Both displacement and stress show signs of premature failure after gradually increasing with deterioration evolution. The stress produces ‘concentration-release’ around the buckling failure. On the whole, the stress variation is earlier than the displacement variation, indicating that the stress monitoring is more effective. The core of stress monitoring is to determine the ‘key section’. For the ‘deterioration-buckling’ bank slope, the sharp increase of stress at the ‘deflection section’ of the front edge can be an important characterization of the critical instability of the bank slope. The trailing edge pushing always exists in the evolution process of ‘deterioration buckling’, which is the premise of bank slope catastrophe failure. However, the dominant factor of bank slope instability is the continuous deterioration of the rock mass in the hydro-fluctuation belt. The Qingshi #6 slope is currently in the process of evolution toward ‘strong bending uplift’, it may gradually evolve from a stable/basically stable state to an understable state, due to the continuous deterioration of the rock mass in the hydro-fluctuation belt.
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spelling doaj.art-bd766589cbf04d58bea4003089ec37eb2022-12-22T02:45:30ZengSCIENCE PRESS , 16 DONGHUANGCHENGGEN NORTH ST, BEIJING, PEOPLES R CHINA, 100717Rock and Soil Mechanics1000-75982022-09-014392568258010.16285/j.rsm.2021.7009Deterioration-buckling failure mechanism of consequent bedding limestone bank slope in Three Gorges Reservoir areaYAN Guo-qiang0YIN Yue-ping1HUANG Bo-lin 2HU Lei31. Faculty of Engineering, China University of Geosciences, Wuhan, Hubei 430074, China2. China Institute of Geological Environment Monitoring, Beijing 100081, China 3. Hubei Key Laboratory of Disaster Prevention and Mitigation, China Three Gorges University, Yichang, Hubei 443002, China 3. Hubei Key Laboratory of Disaster Prevention and Mitigation, China Three Gorges University, Yichang, Hubei 443002, China In the Wuxia section of the Three Gorges Reservoir area, it is found that there are many deformation signs of sliding-bending along the bedding bank slope, and the cyclic fluctuation of reservoir water worsens the deterioration and instability of the bank leading edge. Taking Qingshi #6 slope in the Wuxia section as an example, an laboratory generalized model is constructed to study the catastrophe mechanism of bedding limestone bank slope under the deterioration of rock mass in hydro-fluctuation belt. The research shows that: the bank slope is in a stable state as a whole for a long time before impoundment. After impoundment, with the deterioration aggravation of rock mass, the bank slope deformation intensifies until buckling failure. The deterioration of rock mass shortens the instability process of ‘deterioration-buckling’. Kinematic analysis shows that the peak velocity of the same rock stratum is similar during buckling failure. The movement characteristics of the rear part of the ‘buckling point’ of rock mass are relatively consistent, but the front part is relatively discrete. The buckling failure is the turning point and apex of bank slope energy release. Both displacement and stress show signs of premature failure after gradually increasing with deterioration evolution. The stress produces ‘concentration-release’ around the buckling failure. On the whole, the stress variation is earlier than the displacement variation, indicating that the stress monitoring is more effective. The core of stress monitoring is to determine the ‘key section’. For the ‘deterioration-buckling’ bank slope, the sharp increase of stress at the ‘deflection section’ of the front edge can be an important characterization of the critical instability of the bank slope. The trailing edge pushing always exists in the evolution process of ‘deterioration buckling’, which is the premise of bank slope catastrophe failure. However, the dominant factor of bank slope instability is the continuous deterioration of the rock mass in the hydro-fluctuation belt. The Qingshi #6 slope is currently in the process of evolution toward ‘strong bending uplift’, it may gradually evolve from a stable/basically stable state to an understable state, due to the continuous deterioration of the rock mass in the hydro-fluctuation belt. http://rocksoilmech.whrsm.ac.cn/EN/10.16285/j.rsm.2021.7009physical model testrock mass deteriorationconsequent bedding limestone bank slopedeterioration-bucklingwuxia section of the three gorges reservoir
spellingShingle YAN Guo-qiang
YIN Yue-ping
HUANG Bo-lin
HU Lei
Deterioration-buckling failure mechanism of consequent bedding limestone bank slope in Three Gorges Reservoir area
Rock and Soil Mechanics
physical model test
rock mass deterioration
consequent bedding limestone bank slope
deterioration-buckling
wuxia section of the three gorges reservoir
title Deterioration-buckling failure mechanism of consequent bedding limestone bank slope in Three Gorges Reservoir area
title_full Deterioration-buckling failure mechanism of consequent bedding limestone bank slope in Three Gorges Reservoir area
title_fullStr Deterioration-buckling failure mechanism of consequent bedding limestone bank slope in Three Gorges Reservoir area
title_full_unstemmed Deterioration-buckling failure mechanism of consequent bedding limestone bank slope in Three Gorges Reservoir area
title_short Deterioration-buckling failure mechanism of consequent bedding limestone bank slope in Three Gorges Reservoir area
title_sort deterioration buckling failure mechanism of consequent bedding limestone bank slope in three gorges reservoir area
topic physical model test
rock mass deterioration
consequent bedding limestone bank slope
deterioration-buckling
wuxia section of the three gorges reservoir
url http://rocksoilmech.whrsm.ac.cn/EN/10.16285/j.rsm.2021.7009
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AT huangbolin deteriorationbucklingfailuremechanismofconsequentbeddinglimestonebankslopeinthreegorgesreservoirarea
AT hulei deteriorationbucklingfailuremechanismofconsequentbeddinglimestonebankslopeinthreegorgesreservoirarea